Cloud Identification
Low Level Clouds - V
Stratocumulus (hybrids of layered stratus and cellular cumulus)
When the atmosphere has both convective and advective forces happening
at the same time, stratocumulus clouds result. Stratocumulus clouds often occur in
a shallow layer of unstable air near the surface that is overlain by stable air.
Stratocumulus are frequent in certain geographic regions, such as along coasts and
in valleys. Cold air passing over warmer water will also produce stratocumulus. This
is why this cloud is common in the winter near the Great Lakes. Stratocumulus also
accompany cold fronts. When associated with a large weather system, stratocumulus are
often the last cloud to appear before the skies clear.
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Identify Stratocumulus Clouds in Satellite Images
The first satellite image is a visible image using reflected light, the second satellite image is an IR image that measures thermal energy.
Use your mouse or finger and slide across the image to fade between the different images.
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